ch. 4- rocks
DESCRIPTION
Ch. 4- Rocks . Rock : solid mixture of crystals of 1 or more minerals. Characteristics to Classify Rocks . Composition : minerals that make up rock Texture : size, shape, and positions of the grains in rock 1. Fine grained 2. Medium grained 3. Coarse grained. Rock Cycle . - PowerPoint PPT PresentationTRANSCRIPT
Ch. 4- Rocks
• Rock: solid mixture of crystals of 1 or more minerals.
Characteristics to Classify Rocks
• Composition: minerals that make up rock
• Texture: size, shape, and positions of the grains in rock
• 1. Fine grained• 2. Medium grained• 3. Coarse grained
Rock Cycle • Rock cycle is a continual process
by which new rock form from old rock material.
• Processes that shape the surface of the earth: –Weathering– Erosion–Deposition– Uplift
Sedimentary Rock• Form by process of erosion and
weathering to break down other rocks into sediment which is deposited and compacted
Sedimentary Rock• 3 types of sedimentary rock: – 1. Clastic Sedimentary rock- forms
when rock or mineral fragments are cemented together • Classified by size of fragments they are
made of – 2. Chemical Sedimentary rock: form
from solutions of dissolved minerals and water• Crystallize out of solutions- EX- salt
water
– 3. Organic- forms from remains of plants and animals that cement together• EX- limestone
• Sedimentary structures include:– Ripple marks–Mud cracks– Raindrop impressions
Metamorphic Rock• “meta”= change• “morphos”= shape
• Structure, texture, or composition has changed.
• Most common metamorphic change is caused by pressure
Texture of Metamorphic Rock
• Foliated metamorphic rocks- mineral crystals aligned in planes or bands
• Non-foliated metamorphic rocks- not aligned crystals
• Metamorphic structures are caused by deformation.
2 Types of Metamorphism
• 1. Contact Metamorphism: when a rock comes on contact w/ magma or heat from magma.–Only occurs next to igneous
intrusions• 2. Regional Metamorphism:
enormous pressure b/w deeply buried rock or when crusts collide causing heat and the pressure to change rock.
Igneous Rock• Igneous comes from the Latin
word “fire”• Form when magma cools and
hardens• Texture is determined by rate at
which the rock cools
• Igneous rock that solidifies at Earth’s surface- extrusive
• Igneous rock that solidifies within earth’s surface- intrusive
• Common shapes of intrusive igneous bodies: – Batholiths– Stocks– Sills–Dikes
• Classifying Igneous Rock:• 1. Felsic:– Light colored– Less dense– Rich in silicon, aluminum, sodium,
potassium• 2. Mafic:–Dark colored–More dense– Rich in iron, magnesium, calcium